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Correction to: Contributions to Mineralogy and Petrology (2024) 179:44https://doi.org/10.1007/s00410-024-02125-0
In the original publication, figures 7 and 8 have been incorrectly published. The corrected figures are:
Misorientation axis distributions for diopside-plagioclase pairs. a Theoretical uniform misorientation axis distribution, showing the diopside reference frame as poles to planes (in red) and the plagioclase reference frame as crystallographic axes (in blue). b–g Correlated misorientation axis distribution for all samples: b SZ-N-018-1 (vermicular), c L-042-1 (vermicular), d L-042-2 (vermicular), e WP039A-1 (granular), f WP039A-2 (granular), g WP039A-3 (granular). Poles and axes labelled in each diagram correspond to the maxima in the respective plots
Misorientation axis distributions of vermicular symplectites for specific angle ranges: a SZ-N-018-1 (vermicular); 77–103°; b SZ-N-018-1 (vermicular); 140–170°; c L-042-1 (vermicular); 73–114°; d L-042–2 (vermicular); 135–160°
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Zertani, S., Morales, L.F.G. & Menegon, L. Correction to: Omphacite breakdown: nucleation and deformation of clinopyroxene-plagioclase symplectites. Contrib Mineral Petrol 179, 78 (2024). https://doi.org/10.1007/s00410-024-02140-1
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DOI: https://doi.org/10.1007/s00410-024-02140-1